{"public_id":"cl_973e76b3138e3ee39d666e86c5d10d29","status":"active","superseded_by_public_id":null,"corpus_id":129108694,"text":"The drowned shelves fringing the Hawaiian Islands are thought to have been produced by isostatic subsidence related to overloading of the crust, with crustal rigidity and elasticity causing depression beyond the limits of the load to form the Hawaiian Deep.","confidence":0.93,"paper":{"corpus_id":129108694,"title":"Hawaiian Swell, Deep, and Arch, and Subsidence of the Hawaiian Islands","url":"https://sah.borca.ai/papers/129108694"},"contributors":[{"id":1,"public_id":"12632b8b5f","public_label":"Anonymous (12632b8b5f)","roles":["extraction"],"url":"https://sah.borca.ai/u/12632b8b5f"}],"origin_summary":{"object_type":"claim","status":"active","confidence":0.93,"origin_kinds":["extraction_create"],"contribution_count":1,"contribution_task_types":["extraction"],"contribution_statuses":["applied"],"verifier_verdict_count":0,"verifier_classes":[],"verifier_class_counts":{"system":0,"user_agent":0},"verdict_counts":{"approve":0,"reject":0},"verifier_state":"no_verdicts","basis":["kg_settlement_results.decision_payload.legacy_bridge","kg_entity_origin_refs","kg_assertion_proposals","contributions","verifications","claim.status","claim.confidence"],"limits":["ledger provenance is aggregated; raw contribution and verifier audit rows are not expanded","entity matching uses settlement bridge refs and edge commands"]},"concepts":[{"public_id":"co_113b948793993b1ad383ea22ef4774af","name":"drowned shelves","description":"Submerged coastal shelves around the Hawaiian Islands interpreted as former shelves now below sea level.","types":["coastal feature"],"url":"https://sah.borca.ai/concepts/co_113b948793993b1ad383ea22ef4774af"},{"public_id":"co_72b8a6d06870c77155682e6142d18ac3","name":"Hawaiian Deep","description":"A depressed area at the base of much of the Hawaiian Ridge.","types":["geologic feature"],"url":"https://sah.borca.ai/concepts/co_72b8a6d06870c77155682e6142d18ac3"},{"public_id":"co_ad72d47e3d847205694e27d8f0416bb0","name":"isostatic subsidence","description":"Downward adjustment of the crust in response to loading or mass redistribution.","types":["geologic process"],"url":"https://sah.borca.ai/concepts/co_ad72d47e3d847205694e27d8f0416bb0"}],"related_claims":[],"url":"https://sah.borca.ai/claims/cl_973e76b3138e3ee39d666e86c5d10d29"}